Tsunami detection by GPS-derived ionospheric total electron content

Abstract To unravel the relationship between earthquake and tsunami using ionospheric total electron content (TEC) changes, we analyzed two Chilean tsunamigenic subduction earthquakes: the 2014 Pisagua Mw 8.1 and the 2015 Illapel Mw 8.3. During the Pisagua earthquake, the TEC changes were detected a...

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Main Authors: Mahesh N. Shrivastava, Ajeet K. Maurya, Gabriel Gonzalez, Poikayil S. Sunil, Juan Gonzalez, Pablo Salazar, Rafael Aranguiz
Format: Article
Language:English
Published: Nature Publishing Group 2021-06-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-92479-3
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spelling doaj-39e14d36277e4186b70dd388da7ff43c2021-06-27T11:33:33ZengNature Publishing GroupScientific Reports2045-23222021-06-0111111310.1038/s41598-021-92479-3Tsunami detection by GPS-derived ionospheric total electron contentMahesh N. Shrivastava0Ajeet K. Maurya1Gabriel Gonzalez2Poikayil S. Sunil3Juan Gonzalez4Pablo Salazar5Rafael Aranguiz6Department of Geological Sciences, Universidad Catolica del NorteDepartment of Physics, Doon UniversityDepartment of Geological Sciences, Universidad Catolica del NorteDepartment of Marine Geology and Geophysics, School of Marine Sciences, Cochin University of Science and TechnologyNational Research Center for Integrated Natural Disaster ManagementDepartment of Geological Sciences, Universidad Catolica del NorteNational Research Center for Integrated Natural Disaster ManagementAbstract To unravel the relationship between earthquake and tsunami using ionospheric total electron content (TEC) changes, we analyzed two Chilean tsunamigenic subduction earthquakes: the 2014 Pisagua Mw 8.1 and the 2015 Illapel Mw 8.3. During the Pisagua earthquake, the TEC changes were detected at the GPS sites located to the north and south of the earthquake epicenter, whereas during the Illapel earthquake, we registered the changes only in the northward direction. Tide-gauge sites mimicked the propagation direction of tsunami waves similar to the TEC change pattern during both earthquakes. The TEC changes were represented by three signals. The initial weaker signal correlated well with Acoustic Rayleigh wave (AWRayleigh), while the following stronger perturbation was interpreted to be caused by Acoustic Gravity wave (AGWepi) and Internal Gravity wave (IGWtsuna) induced by earthquakes and subsequent tsunamis respectively. Inevitably, TEC changes can be utilized to evaluate earthquake occurrence and tsunami propagation within a framework of multi-parameter early warning systems.https://doi.org/10.1038/s41598-021-92479-3
collection DOAJ
language English
format Article
sources DOAJ
author Mahesh N. Shrivastava
Ajeet K. Maurya
Gabriel Gonzalez
Poikayil S. Sunil
Juan Gonzalez
Pablo Salazar
Rafael Aranguiz
spellingShingle Mahesh N. Shrivastava
Ajeet K. Maurya
Gabriel Gonzalez
Poikayil S. Sunil
Juan Gonzalez
Pablo Salazar
Rafael Aranguiz
Tsunami detection by GPS-derived ionospheric total electron content
Scientific Reports
author_facet Mahesh N. Shrivastava
Ajeet K. Maurya
Gabriel Gonzalez
Poikayil S. Sunil
Juan Gonzalez
Pablo Salazar
Rafael Aranguiz
author_sort Mahesh N. Shrivastava
title Tsunami detection by GPS-derived ionospheric total electron content
title_short Tsunami detection by GPS-derived ionospheric total electron content
title_full Tsunami detection by GPS-derived ionospheric total electron content
title_fullStr Tsunami detection by GPS-derived ionospheric total electron content
title_full_unstemmed Tsunami detection by GPS-derived ionospheric total electron content
title_sort tsunami detection by gps-derived ionospheric total electron content
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-06-01
description Abstract To unravel the relationship between earthquake and tsunami using ionospheric total electron content (TEC) changes, we analyzed two Chilean tsunamigenic subduction earthquakes: the 2014 Pisagua Mw 8.1 and the 2015 Illapel Mw 8.3. During the Pisagua earthquake, the TEC changes were detected at the GPS sites located to the north and south of the earthquake epicenter, whereas during the Illapel earthquake, we registered the changes only in the northward direction. Tide-gauge sites mimicked the propagation direction of tsunami waves similar to the TEC change pattern during both earthquakes. The TEC changes were represented by three signals. The initial weaker signal correlated well with Acoustic Rayleigh wave (AWRayleigh), while the following stronger perturbation was interpreted to be caused by Acoustic Gravity wave (AGWepi) and Internal Gravity wave (IGWtsuna) induced by earthquakes and subsequent tsunamis respectively. Inevitably, TEC changes can be utilized to evaluate earthquake occurrence and tsunami propagation within a framework of multi-parameter early warning systems.
url https://doi.org/10.1038/s41598-021-92479-3
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